The Gutenberg Discontinuity is found above the earth layer called the outer core. This boundary line, which separates the outer core from the lower mantle, is approximately 1798 miles below the Earth's surface.
The Gutenberg Discontinuity is found between the Earth's lower mantle and the Earths outer core. It is about 1800 miles below the surface of the earth.
The Gutenberg discontinuity is found at the base of the mantle and marks the core mantle boundary.
The Gutenberg Discontinuity is found at the base of the mantle.
mantle
The Gutenberg discontinuity is found directly above the outer core.
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
Crust
Well, the crust is the top layer of the earth and then the moho, upper mantle, transition zone, lower mantle, Gutenberg discontinuity, outer core and then the inner core...theres really nothing eles.
The sial layer has a lighter density than the sima layer, which is due to increased amount of aluminium, and decreased amount of iron and magnesium.
The Gutenberg discontinuity is actually found at the base of the mantle, not the lithosphere.
The Gutenberg discontinuity is found directly above the outer core.
The Gutenberg discontinuity was discovered by a German geophysicist named Beno Gutenberg in 1913.Gutenberg find out that it is the boundary that seperates the two layers.The gutenberg layer is 1500 km thick.
I think there is a layer called the Gutenberg Discontinuity named after a german seismologist named Beno Gutenberg between lower mantle and outer core.
The Moho , short for Mohorovicic discontinuity , is about 7 kilometers below the floor of the ocean and the MANTLE is the layer immediately beneath the Moho !
The boundary between the mantle and the core is called the core-mantle boundary and also The Gutenberg Discontinuity which marks the upper boundary of the D'' (D Double Prime) layer.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.
The D" layer (pronounced D double prime layer) forms the base of the Earth's lower mantle. Below this lies the outer core. This boundary zone is marked by a seismic discontinuity known as the Gutenberg discontinuity.
The Gutenberg discontinuity is located approximately 2,900 kilometers below the Earth's surface. At this depth, temperatures can reach up to 4,000 degrees Celsius (7,200 degrees Fahrenheit).
Gutenburg Discontinuity
Crust
Well, the crust is the top layer of the earth and then the moho, upper mantle, transition zone, lower mantle, Gutenberg discontinuity, outer core and then the inner core...theres really nothing eles.